云开池垌志留纪辉长岩体的年代学、地球化学特征及构造意义

徐畅; 王岳军; 张玉芝; 徐文景; 甘成势

doi:10.3799/dqkx.2018.592

云开池垌志留纪辉长岩体的年代学、地球化学特征及构造意义

doi: 10.3799/dqkx.2018.592

徐畅^1,,
王岳军^1,2,
张玉芝^1,2, ,,
徐文景^1,2,
甘成势^1,2

1.
中山大学地球科学与工程学院, 广东广州 510275
2.
广东省地球动力作用与地质灾害重点实验室, 广东广州 510275

基金项目:

广东省自然科学基金项目 2018B030312007

国家自然科学基金项目 U1701641

国家自然科学基金项目 41830211

详细信息

作者简介:
徐畅(1996-), 男, 从事地质学方面的学习和研究

通讯作者:
张玉芝

中图分类号: P595
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出版历程
- 收稿日期: 2018-04-23
- 刊出日期: 2019-04-15

Geochronological and Geochemical Constraints of Chidong Silurian Gabbroic Pluton in Yunkai Domain and Its Tectonic Implications

Xu Chang^1
,,
Wang Yuejun^1,2,
Zhang Yuzhi^{1,2
, ,},
Xu Wenjing^1,2,
Gan Chengshi^1,2

1.
School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510275, China
2.
Guangdong Provincial Key Laboratory of Geodynamics and Geohazards, Guangzhou 510275, China

摘要

摘要: 华南陆块早古生代的构造属性是华南地质研究争论的焦点，主要有洋-陆俯冲/碰撞和陆内构造两种观点之争.而华南陆块早古生代岩浆岩的报道以花岗质岩石为主，对构造指示意义更为明确的同期镁铁质岩浆岩则研究较少，且对已发现的少量早古生代镁铁质岩浆岩的岩石成因也颇具争议.为了更好地限定华南早古生代的构造属性，对云开地区新近识别出的池垌辉长岩体开展了详细的野外地质、年代学和地球化学研究.其SIMS锆石U-Pb年代学测试得到其²⁰⁶Pb/²³⁸U加权平均年龄为433.9±1.5 Ma，代表其结晶年龄.样品具较低的SiO₂含量（47.81%~48.83%），高的MgO含量（13.02%~14.65%）、Cr含量（278×10^-6~356×10^-6）和Ni含量（120×10^-6~184×10^-6），富集大离子亲石元素、亏损高场强元素.（⁸⁷Sr/⁸⁶Sr）_i=0.708 5~0.710 7，ε_Nd（t）=-6.0~-8.2，显示EMⅡ型富集地幔的Sr-Nd同位素特征.结合区域Lu-Hf同位素、古生物、古水流等地质资料，云开地区志留纪时期发育一个受古老俯冲交代作用影响的地幔楔，该地幔楔源区在华南广西运动期间才受到热扰动而部分熔融.认为池垌辉长岩是在早古生代华南陆内造山后的伸展背景下由古老俯冲交代地幔楔熔融而成的产物.
- 华南陆块 /
- 云开地块 /
- 早古生代 /
- 池垌辉长岩 /
- 陆内造山 /
- 地球化学
Abstract: The geodynamic mechanisms of the Early Paleozoic orogeny in the South China block (SCB) remain highly debated, and two major models involving subduction-collision orogeny and intra-continental orogeny have been proposed. The Early Paleozoic granitic rocks are widely developed in the eastern SCB and the synchronous mafic rocks have recently been reported.However, the petrogenesis of these Early Paleozoic mafic rocks are still controversial, thus hindering our understanding for the Early Paleozoic tectonic setting. In this study, it presents new petrographic, geochronological and geochemical data for the Chidong gabbroic pluton in the Yunkai domain.The representative sample for the gabbric pluton yields a SIMS zircon U-Pb age of 433.9±1.5 Ma (MSWD=0.18). They have SiO₂ of 47.81%-48.83%, MgO of 13.02%-14.65%, Cr of 278×10^-6-356×10^-6 and Ni of 120×10^-6-184×10^-6.They are enriched in large ion lithophile elements with significantly negative Nb-Ta and Ti anomalies.These samples show EMⅡ-like geochemical affinities with high initial ⁸⁷Sr/⁸⁶Sr ratios (0.708 5 to 0.710 7) and low ε_Nd(t) values (-6.0 to -8.2), suggestive of derivation from a paleosubduction-modified wedge beneath the Yunkai Domain. The wedge was undisturbed until Silurian and the Kwangsian igneous rocks in the SCB were associated with the intra-continental orogenism rather than the subduction and subsequent collision.
- South China block /
- Yunkai Domain /
- Chidong gabbroic pluton /
- intra-continental orogeny /
- geochemistry /

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图 1 信宜-罗定地区地质概况及采样点位置

Fig. 1. Geological sketch of Xinyi-Luoding with the sampling location

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图 2 池垌辉长岩样品(CD-1)的SIMS锆石U-Pb定年谐和图(a)、年龄加权平均图(b)和CL图像(c)

Fig. 2. Concordia diagram of SIMS zircon U-Pb data for the Chidong gabbroic sample (CD-1) (a), inserts note the recalculated weighted mean ²⁰⁶Pb/²³⁸U ages (b) and the respective cathodoluminescenece images for zircons (c)

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图 3 池垌辉长岩样品TAS图解(a)和SiO₂-K₂O图解(b)

图a据Wilson(1989)，图b据Morrison(1980)修改

Fig. 3. TAS diagram (a) and SiO₂-K₂O diagram (b) for the Chidong gabbroic samples

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图 4 池垌辉长岩样品稀土元素球粒陨石标准化图解(a)和微量元素原始地幔标准化配分图(b)

球粒陨石、原始地幔、OIB及MORB数据引自Sun and McDonough(1989)

Fig. 4. Chondrite-normalized REE patterns diagram (a) and primitive mantle-normalized spidergram (b) for the Chidong gabbroic samples

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图 5 池垌辉长岩体的(⁸⁷Sr/⁸⁶Sr)_i-ε_Nd(t)图解(a)、La/Nb-Nb/Th图解(b)、Nb×100/Zr-Th×100/Zr图解(c)和Th/Nb-Ba/Nb图解(d)

龙虎岗岩体数据据Wang et al.(2013b)，云炉岩体数据据彭松柏等(2006a)，竹雅岩体和石板岩体数据据彭松柏等(2006a)和周岱等(2017b)

Fig. 5. (⁸⁷Sr/⁸⁶Sr)_i-ε_Nd(t) diagram (a), La/Nb-Nb/Th diagram (b), Nb×100/Zr-Th×100/Zr diagram (c) and Th/Nb-Ba/Nb diagram (d) for the Chidong gabbroic samples

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表 1 池垌辉长岩样品主量元素(%)、微量元素(10^-6)分析结果

Table 1. Major (%) and trace (10^-6) element analytical results for the Chidong gabbroic samples

样号	CD-4	CD-5	CD-8	CD-10	CD-12	CD-15
SiO₂	48.38	48.53	48.83	47.81	47.94	48.05
TiO₂	0.38	0.37	0.34	0.29	0.28	0.43
Al₂O₃	12.98	11.40	12.10	14.28	13.12	11.79
FeO^T	9.52	10.30	9.66	9.38	10.07	10.13
MgO	13.80	14.65	14.13	13.02	13.97	14.32
MnO	0.18	0.20	0.18	0.17	0.19	0.19
CaO	7.63	8.21	7.96	8.99	8.51	8.90
K₂O	1.34	0.96	1.19	1.17	0.90	0.62
Na₂O	0.82	0.72	1.06	1.08	0.97	0.98
P₂O₅	0.02	0.03	0.02	0.01	0.01	0.02
L.O.I	3.35	2.92	2.94	2.21	2.35	2.91
Total	99.45	99.44	99.49	99.47	99.43	99.46
Mg^#	72.3	71.9	72.5	71.4	71.4	71.8
Sc	39.6	43.1	41.3	38.3	38.5	42.5
V	188	203	185	175	173	209
Cr	278	291	292	327	356	278
Co	57.5	63.8	61.7	64.4	64.1	62.5
Ni	135	133	134	175	184	120
Rb	66.1	46.3	62.7	55.8	43.9	30.9
Sr	93.0	85.6	107	153	111	96.5
Y	9.79	9.31	9.32	7.76	7.10	9.65
Zr	24.8	23.9	28.4	18.4	18.9	32.5
Nb	1.22	1.39	1.26	0.97	0.79	1.30
Ba	120	102	104	120	97.4	63.6
La	3.25	4.24	4.09	3.17	2.79	3.52
Ce	6.89	8.42	8.08	5.62	5.12	7.25
Pr	1.00	1.08	1.06	0.81	0.71	0.96
Nd	3.95	4.72	4.59	3.40	3.10	3.97
Sm	1.14	1.15	1.17	0.89	0.81	1.16
Eu	0.34	0.35	0.33	0.31	0.28	0.36
Gd	1.42	1.38	1.41	1.14	1.04	1.39
Tb	0.25	0.24	0.25	0.20	0.18	0.26
Dy	1.55	1.51	1.50	1.23	1.11	1.59
Ho	0.33	0.33	0.33	0.27	0.25	0.34
Er	0.99	0.98	0.97	0.81	0.77	1.02
Tm	0.15	0.15	0.15	0.12	0.11	0.15
Yb	0.96	0.98	0.98	0.81	0.77	1.00
Lu	0.14	0.15	0.15	0.12	0.12	0.15
Hf	0.70	0.77	0.75	0.53	0.53	0.84
Ta	0.10	0.12	0.10	0.11	0.06	0.09
Pb	3.56	14.5	9.23	3.28	2.85	4.19
Th	0.98	1.01	1.14	0.71	0.76	1.05
U	0.23	0.26	0.36	0.21	0.17	0.28

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表 2 池垌辉长岩样品Sr-Nd同位素分析结果

Table 2. Sr-Nd isotopic results for the Chidong gabbroic samples

样号	⁸⁷Rb/⁸⁶Sr	⁸⁷Sr/⁸⁶Sr	±2σ	(⁸⁷Sr/⁸⁶Sr)_i	¹⁴⁷Sm/¹⁴⁴Nd	¹⁴³Nd/¹⁴⁴Nd	±2σ	(¹⁴³Nd/¹⁴⁴Nd)_t	ε_Nd(t)
CD-10	1.056	0.717 185	14	0.710 660	0.158	0.512 221	18	0.511 772	-6.0
CD-4	2.058	0.721 194	14	0.708 477	0.174	0.512 153	17	0.511 658	-8.2
注：采用加权平均年龄434 Ma求得样品Sr、Nd同位素的初始比值.参数采用λ(⁸⁷Rb)=1.42×10^-11(a^-1)，λ(¹⁴⁷Sm)=6.54×10^-12(a^-1) (Lugmair and Marti, 1978)，(¹⁴³Nd/¹⁴⁴Nd)_{CHUR, 现在}=0.512 638(Goldstein et al., 1984)，(¹⁴⁷Sm/¹⁴⁴Nd)_{CHUR, 现在}=0.196 7(Peucat et al., 1988).

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